Dataset - B2FIND

(Table 4) Element ratios in sedimentary deposits at DSDP Leg 55 Holes

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(Table 5) Ratios between principal elements of the sedimentary deposits at DS...

Empty cells = no values of trace-element contents.

(Table 4) Interrelations among major elements at DSPD Leg 55 Holes

Empty cells mean no data.

(Table 4) Ratios of Ti, Al, Fe, and Mn for sediments at DSDP Legs 56-57 Holes

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(Table 2) Bulk geochemistry of sediments at DSDP Hole 62-464

= Value below detection limit; total iron was calculated as Fe2O3, and total manganese as Mn3O4; CaCO3 was calculated using the total CaO.

(Table 3) Major element content in different bulk sediment fractions from ODP...

Sediment depth is given in mcd. Age model after Channell et al. (2003, datasets: doi:10.1594/PANGAEA.717737). All data are normalized to initial sample bulk weight.

(Table T3) Metal concentrations of ODP Leg 194 sites and survey sites crusts

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(Table S1) Geochemistry of ODP Hole 157-953C lavas

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(Table 1) Olivine phenocryst and bulk rock Sr, Nd and Pb isotopic composition...

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(Table 3) Major and minor element composition of ferromanganese nodules and c...

All sample concentrations expressed in weight percent on 110°C dried basis.

(Table 3) Chemical and mineralogical composition of the deposits

Mineralogy: + + = abundant, + = present, t = trace, - = not detected

(Table 1) Chemistry of two samples of the red weathered layer at DSDP Hole 55...

One argument for the subaerial formation of Nintoku Seamount in the Emperor chain is the occurrence of a red claystone interlayered between two basalt flows in Hole 432A....